67 results were found for WA 0821 1305 0400 Jual Material Geoteknik Geomat Berkualitas Ciamis Jawa Barat.

Results:

• 31. A large landslide falls in Hítardalur valley

  displacements and might be an old landslide deposit. The displaced material is a mixture of e.g. rock debris, scree from the lower part of the hillside, swamp soil and sediments from ancient lakes on the valley bottom. A preliminary estimate of the volume of the slide is 10–20 million m3. The area of the debris tongue is ca. 1,5 km2 and the debris is up to 20–30 m thick. The thickness is 5–10 m in many /about-imo/news/a-large-landslide-falls-in-hitardalur-valley

• 32. Bárðarbunga and Holuhraun - overview

  A list of links to the relevant web-material 20.8.2014 An overview of the Bárðarbunga seismic events and the Holuhraun eruption, 2014 - 2015, is given here with notes, factsheets and observations. New material was added to the top of each monthly article. Combined /earthquakes-and-volcanism/articles/nr/2947

• 33. Pyroclastic flow

  a small amount of their heat to the atmosphere when the currents form. The temperature of the current can vary from 100°C up to 800°C. Depending on the density PDCs can be categorized into two groups. If the column contains a lot of solid material while it collapses it is called pyroclastic flows, however, if the quantity of solid material is low compared to the gases it is called a pyroclastic /volcanoes/volcanic-hazards/pyroclastic-flow/

• 34. A large landslide falls in Hítardalur valley

  displacements and might be an old landslide deposit. The displaced material is a mixture of e.g. rock debris, scree from the lower part of the hillside, swamp soil and sediments from ancient lakes on the valley bottom. A preliminary estimate of the volume of the slide is 10–20 million m3. The area of the debris tongue is ca. 1,5 km2 and the debris is up to 20–30 m thick. The thickness is 5–10 m in many /about-imo/news/a-large-landslide-falls-in-hitardalur-valley/

• 35. Bárðarbunga and Holuhraun - overview

  A list of links to the relevant web-material 20.8.2014 An overview of the Bárðarbunga seismic events and the Holuhraun eruption, 2014 - 2015, is given here with notes, factsheets and observations. New material was added to the top of each monthly article. Combined /earthquakes-and-volcanism/articles/nr/2947/

• 36. Rockslide into Askja caldera

  rim might still be unstable and more material might fall into the lake. The situation was reviewed this morning by scientists from IMO, the University of Iceland and the Civil Protection System of the Icelandic police. Scientists are now on the way to Askja to evaluate the impact of the rockslide and any remaining hazards. Traffic in the area is restricted until further notice. The responsible /about-imo/news/nr/2919

• 37. Hekla

  and explosive eruptions. The period 9000-7000 years ago was dominated by effusive basaltic volcanism, the period 7000-3000 years ago was characterized by infrequent but large explosive silicic eruptions at the central volcano and effusive basaltic eruptions. In the last 3000 years a mixture of both lava and tephra has been dominating.The chemical composition of erupted material from Hekla /volcanoes/about-volcanoes/hekla/

• 38. The weather in Iceland 2007

  and recurrent fierce wind-storms caused some material damages and interrupted air and land communication on several occasions. Except for a two-week period in January, the snow cover in 2007 was very light compared to the long-term mean (1961-1990). Documents Other Annual summaries This article, The weather in Iceland 2007, can be read here in pdf (0.3 Mb /about-imo/news/2008/nr/1205

• 39. The weather in Iceland 2007

  and recurrent fierce wind-storms caused some material damages and interrupted air and land communication on several occasions. Except for a two-week period in January, the snow cover in 2007 was very light compared to the long-term mean (1961-1990). Documents Other Annual summaries This article, The weather in Iceland 2007, can be read here in pdf (0.3 Mb /about-imo/news/nr/1205

• 40. Latest observations at Eyjafjallajökull

  days. A volcanic crater has formed in the south-western corner of the cauldron. Erupted material from the vent continues to accumulate on the flanks of the crater. The rim of the volcanic crater is ~50 m lower than the surrounding ice cauldron. Volcanic spatter was observed from the vent, with ejected lava reaching heights of 100-200 m. Unstable plumes of ash rise regularly from the vent. Lava /about-imo/news/nr/1891